缅甸锡钨矿床特征及找矿前景浅析  

Characteristics and prospecting prospects of tin tungsten deposits in Myanmar

作　　者：莫火华 刘孝滨 杨斌[1] MO Huo-hua;LIU Xiao-bin;YANG Bin(Gannan Geological Party,Bureau of Geology and Mineral Exploration and Development of Jiangxi Province,Ganzhou 341000,China)

机构地区：[1]江西省地质矿产勘查开发局赣南地质调查大队,江西赣州341000

出　　处：《世界有色金属》2020年第23期71-72,共2页World Nonferrous Metals

摘　　要：缅甸地处于冈瓦纳和劳亚两大古陆的边缘交汇部位,区内中-新生代弧后岩浆作用极为发育,形成了巨大的锡钨花岗岩带,是东南亚中南半岛锡矿带重要组成部分,区内成矿地质条件优越,具较好找矿潜力。Myanmar is located at the intersection of Gondwana and Laoya.The Mesozoic Cenozoic back arc magmatism in the area is extremely developed,forming a huge tin tungsten granite belt.It is an important part of the tin ore belt in the Indochina Peninsula of Southeast Asia.The metallogenic geological conditions in the area are superior,with good prospecting potential.

关 键 词：钨锡矿 矿床地质特征 找矿前景 

分 类 号：P618.77[天文地球—矿床学]